Moisture, Pore Space, and Bulk Density Changes in Frozen Soil1
- A. W. Krumbach and
- D. P. White2
In the upper 15 inches of 2 frozen loam soils, one bare and one under alfalfa, moisture contents usually exceeded prefreeze field maximum. Total pore space was always above that before freezing; bulk density was predominantly less than the lowest expected prefreeze bulk density. Moisture changes in the frozen soils are attributed solely to internal moisture movement.Please view the pdf by using the Full Text (PDF) link under 'View' to the left.
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